Determination of ancient erosion by zircon morphology and investigations on zoned tourmaline in Kőszeg-Rechnitz Window (Western Hungary)
The rocks exposed in the Kőszeg-Rechnitz Window in Western Hungary and Austria belong to the Penninic unit of the Alps. The investigated rocks are of sedimentary origin, mostly graphitic chlorite-muscovite phyllites and quartzphyllites. The latter contains significant amounts of detrital zircon and...
Elmentve itt :
| Szerző: | |
|---|---|
| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1987
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| Sorozat: | Acta mineralogica-petrographica
29 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24754 |
| LEADER | 01609nab a2200217 i 4500 | ||
|---|---|---|---|
| 001 | acta24754 | ||
| 005 | 20220726133416.0 | ||
| 008 | 161017s1987 hu o 0|| eng d | ||
| 022 | |a 0365-8066 | ||
| 040 | |a SZTE Egyetemi Kiadványok Repozitórium |b hun | ||
| 041 | |a eng | ||
| 100 | 1 | |a Demény Attila | |
| 245 | 1 | 0 | |a Determination of ancient erosion by zircon morphology and investigations on zoned tourmaline in Kőszeg-Rechnitz Window (Western Hungary) |h [elektronikus dokumentum] / |c Demény Attila |
| 260 | |a University of Szeged, Department of Mineralogy, Geochemistry and Petrology |b Szeged |c 1987 | ||
| 300 | |a 13-26 | ||
| 490 | 0 | |a Acta mineralogica-petrographica |v 29 | |
| 520 | 3 | |a The rocks exposed in the Kőszeg-Rechnitz Window in Western Hungary and Austria belong to the Penninic unit of the Alps. The investigated rocks are of sedimentary origin, mostly graphitic chlorite-muscovite phyllites and quartzphyllites. The latter contains significant amounts of detrital zircon and tourmaline. Morphology of zircon grains has been preserved during metamorphism and indicates alkaline granite, plagiogranite, monzogranite and garnodiorite source rocks. Electron microprobe investigation on tourmaline grains indicates formation in Ca-poor metapelites and metapsammites without Al-saturated phases. These rocks have shed part of the sediments deposited in the Penninic ocean. | |
| 650 | 4 | |a Természettudományok | |
| 650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
| 695 | |a Kőzettan, Ásványtan, Földtan | ||
| 856 | 4 | 0 | |u http://acta.bibl.u-szeged.hu/24754/1/mineralogica_029_013-026.pdf |z Dokumentum-elérés |